[vc_row][vc_column][vc_column_text] NOC of Groundwater withdrawal from CGWA or State Groundwater Authority is mandatory for all Industries and Infrastructure projects. CGWA has made a panel of Accredited Consultants who understand the
[vc_row][vc_column][vc_column_text] Detailed Guidelines for Abstraction of Saline Ground Water Water having above EC above 5000 µ siemens/cm at 250C is Saline Water. Any user desirous of utilizing saline groundwater is
[vc_row][vc_column][vc_column_text] Guidelines for Ground Water abstraction for bulk water supply As per the new guidelines, all those users abstracting ground water and using it for supply as bulk water supplies
[vc_row][vc_column][vc_column_text] The occurrence and distribution of groundwater are controlled primarily by the geology of the area and the quantum of recharge received by the existing aquifer formations. Thus the alluvial
[vc_row][vc_column][vc_column_text] Water first enters an aquifer through gravity-induced downward movement (percolation), but it also flows in a lateral direction within an aquifer. This flow can occur due to the dip
[vc_row][vc_column][vc_column_text] Regionally, the top surface of the saturated zone is visualized as flat as the top of a table and hence this surface is referred to as the water table.
[vc_row][vc_column][vc_column_text] Sometimes they mean the same, but not always. While the uppermost level (top) of the saturated zone in an unconfined aquifer is the water table, the water level seen
[vc_row][vc_column][vc_column_text] Rainfall (precipitation), an integral part of the hydrological cycle, is the source of all fresh water on the earth. We tend to misjudge the enormous quantity of water brought
[vc_row][vc_column][vc_column_text] From the hydrogeology point of view, rock formations are categorized conveniently as unconsolidated (loose), consolidated (hard) and semi-consolidated. Recent and older alluviums are unconsolidated sedimentary formations, usually as alternate
[vc_row][vc_column][vc_column_text] Groundwater moves through porous rock formations, similar to water flowing through a sponge with interconnected pores. In nature, no space remains empty. Therefore, the pore space within the underground
